The Erdahl plate. Relief from Copernicus GLO-30; rivers and lakes from USGS NHD; watersheds from the USGS Watershed Boundary Dataset; roads and city limits from Census TIGER 2024.
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Erdahl’s center stands about 1,270 ft above sea level. Within three miles the land runs from 1,160 ft to 1,360 ft, a difference of 200 ft: gently rolling country. The highest named summit within 15 miles is Tower Hill, about 1,600 ft, 14 miles southeast.
Under the town center the state geologic map shows Schist of sedimentary protolith, from the Neoarchean, 2.5 to 2.8 billion years old.
The section below crosses 2 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 56×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Felsic-volcanic. Age: Neoarchean, 2.5 to 2.8 billion years old. About 14 mi of the line.
Schist. Age: Neoarchean, 2.5 to 2.8 billion years old. About 11 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale.
Heights from Copernicus GLO-90 (a surface model: it includes buildings and tree canopy); summits from USGS GNIS; rivers from USGS NHDPlus HR; rock from the USGS State Geologic Map Compilation.
A raindrop that lands in Erdahl reaches the Gulf of America by way of the Pomme de Terre, the Minnesota and the Mississippi: about 2,220 river miles.
Lake on the way: Lake Pepin.
1,750 miles of the trip are on the Mississippi.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Erdahl; river miles along the main stem, rounded.
